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  2. Equatorial plasma bubble - Wikipedia

    en.wikipedia.org/wiki/Equatorial_plasma_bubble

    Different times of the year and locations have different frequencies of occurrence. In Northern Australia, the most common times are February to April and August to October, when a plasma bubble is expected every night. [1] Plasma bubbles have dimensions around 100 km. [2] Plasma bubbles form after dark when the sun stops ionising the ...

  3. High-frequency Active Auroral Research Program - Wikipedia

    en.wikipedia.org/wiki/High-frequency_Active...

    Balloons cannot reach it because the air is too thin, but satellites cannot orbit there because the air is too thick. Hence, most experiments on the ionosphere give only small pieces of information. HAARP approaches the study of the ionosphere by following in the footsteps of an ionospheric heater called EISCAT near Tromsø, Norway. There ...

  4. WWVB - Wikipedia

    en.wikipedia.org/wiki/WWVB

    WWVB's Colorado location makes the signal weakest on the U.S. east coast, where urban density also produces considerable interference. In 2009, NIST raised the possibility of adding a second time code transmitter, on the east coast, to improve signal reception there and provide a certain amount of robustness to the overall system should weather or other causes render one transmitter site ...

  5. Ionospheric heater - Wikipedia

    en.wikipedia.org/wiki/Ionospheric_heater

    Platteville Atmospheric Observatory, Colorado, USA (stopped ionospheric heater research in 1984 but still operates as an atmospheric observatory). SPEAR (Space Plasma Exploration by Active Radar) [ 5 ] is an installation operated by UNIS (the University Centre in Svalbard ) adjacent to the EISCAT facilities at Longyearbyen in Svalbard , Norway ...

  6. Scientists have spotted unexpected X- and C-shaped ... - AOL

    www.aol.com/scientists-spotted-unexpected-x-c...

    Scientists studying the zone between Earth’s atmosphere and space have spotted unusual X- and C-shaped features that could thwart signals that keep our planet running smoothly.

  7. F region - Wikipedia

    en.wikipedia.org/wiki/F_region

    The density falls off to below 10 4 e/cm 3 at night. The F 1 layer merges into the F 2 layer at night. Though fairly regular in its characteristics, it is not observable everywhere or on all days. The principal reflecting layer during the summer for paths of 2,000 to 3,500 km (1,200 to 2,200 miles) is the F 1 layer. However, this depends upon ...

  8. Ionosphere - Wikipedia

    en.wikipedia.org/wiki/Ionosphere

    Relationship of the atmosphere and ionosphere. The ionosphere (/ aɪ ˈ ɒ n ə ˌ s f ɪər /) [1] [2] is the ionized part of the upper atmosphere of Earth, from about 48 km (30 mi) to 965 km (600 mi) above sea level, [3] a region that includes the thermosphere and parts of the mesosphere and exosphere. The ionosphere is ionized by solar ...

  9. Whoopsie, SpaceX Blew Up Two Rockets and Punched a ... - AOL

    www.aol.com/whoopsie-spacex-blew-two-rockets...

    SpaceX’s rocket explosion in November 2023 created a massive hole in the Earth's ionosphere, providing scientists with a rare opportunity to study its effects.